Logan River, Utah 400 Year Streamflow Reconstructions Allen, E.B.; Rittenour, T.M.; DeRose, R.J.; Bekker, M.F.; Kjelgren, R.; Buckley, B.M. Allen, E.B. Rittenour, T.M. DeRose, R.J. Bekker, M.F. Kjelgren, R. Buckley, B.M. Streamflow Reconstruction hydrology earth science/paleoclimate/climate reconstructions|tree ring (age,null,null,year Common Era,null,climate reconstructions|tree ring,null,null,N,null) earth science/paleoclimate/instrumental (streamflow,null,null,cubic meter per second,Oct-Sep,instrumental,null,null,N,null) earth science/paleoclimate/climate reconstructions|tree ring (streamflow,null,null,cubic meter per second,Oct-Sep,climate reconstructions|tree ring,null,null,N,"""Local"" model that incorporated two Rocky Mountain juniper chronologies located within the basin") earth science/paleoclimate/climate reconstructions|tree ring (streamflow,null,null,cubic meter per second,Oct-Sep,climate reconstructions|tree ring,null,null,N,"""Regional"" model that also included limber pine and pinyon pine chronologies from a larger area") earth science/paleoclimate/climate reconstructions|tree ring (number of samples,null,null,count,null,climate reconstructions|tree ring,null,null,N,number of regional tree ring sample predictors) earth science/paleoclimate/climate reconstructions|tree ring (number of samples,null,null,count,null,climate reconstructions|tree ring,null,null,N,number of local tree ring sample predictors) earth science/paleoclimate/reconstructions (Logan River USGS10109001>LATITUDE 41.7444>LONGITUDE -111.7836) We created six new tree-ring chronologies in northern Utah, which were used with preexisting chronologies from Utah and western Wyoming to reconstruct mean annual flow for the Logan River, the largest tributary of the regionally important Bear River. Two reconstruction models were developed, a "Local" model that incorporated two Rocky Mountain juniper chronologies located within the basin, and a "Regional" model that also included limber pine and pinyon pine chronologies from a larger area. The Local model explained 48.2% of the variability in the instrumental record and the juniper chronologies better captured streamflow variability than Douglas-fir collected within the Logan basin. Incorporating chronologies from the northern and southern margins of the transition zone of the western precipitation dipole increased the skill of the Regional model (r2 = 0.581). We suggest the increased Regional model skill indicates that both nodes of the western precipitation dipole influence northern Utah climate. The importance of Rocky Mountain juniper in both reconstructions of streamflow for this region suggests that future work should target these trees where more traditionally desirable species are not present. The reconstructions provide the first extended record of streamflow in northern Utah. Preinstrumental streamflows (1605-1921) exhibited considerable variability when compared to the instrumental period (1922-2005). Our findings confirm that the inherent uncertainty in contemporary water management and planning in the region is due to hydroclimatic variability that has persisted for at least the last four centuries. STUDY NOTES: The population of semi-arid northern Utah depends on rivers to deliver water stored in mountain snowpack to population centers in the semi-arid valleys of northern Utah. The Logan River is an important tributary to the Bear River, which in turn is the largest stream flowing into the Great Salt Lake. Previously, there were no streamflow reconstructions for the Wasatch Front, and few tree-ring chronologies existed from which reconstructions are typically developed. We used two groups of predictors to model Logan River water year MAF: a Local model that considered predictors within 100 km of the basin boundary, and the Regional model that considered all predictors within an area of putatively similar hydroclimate. Each group of predictors were entered into a stepwise linear regression model ordered by their correlation to Logan River MAF. Predictors were retained based on AIC. The models were verified using a split calibration procedure. The model skill of split and full calibration were assessed using r2, adjusted r2, reduction of error (RE), coefficient of efficiency (CE), and the PRESS statistic. Both models begin in 1605 with the Regional model ending in 2005 while the Local model terminates in 2010. Naturalized mean annual water year flow data used to calibrate the models were obtained from USGS gage 10109001 for the period 1922-2005. Units are cubic meters per second. Sample depth includes all chronologies in a model for a given year. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Allen, E.B. Investigator : Rittenour, T.M. Investigator : DeRose, R.J. Investigator : Bekker, M.F. Investigator : Kjelgren, R. Investigator : Buckley, B.M. 2014-02-08 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/16074 https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/utah/logan2013flow.txt https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/utah/logan2013flow.txt English https://www.ncdc.noaa.gov/paleo/study/16074 https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/utah/logan2013flow.txt Eric B. Allen, Tammy M. Rittenour, R. Justin DeRose, Matthew F. Bekker, Roger Kjelgren, Brendan M. Buckley 2013A tree-ring based reconstruction of Logan River streamflow, northern UtahWater Resources Research49128579-858810.1002/2013WR014273http://onlinelibrary.wiley.com/doi/10.1002/2013WR014273/abstract START YEAR: 1605 AD * END YEAR: 2010 AD -111.7836 41.7444 -111.7836 41.7444